Umba (Tanzania)
Conversion | ||
The course of the Umba |
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Data | ||
location |
Tanzania Kenya |
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River system | Conversion | |
origin | Usambara Mountains | |
Source height | 2000 m | |
muzzle | On the border with Kenya in the Indian Ocean Coordinates: 4 ° 40 ′ 50 " S , 39 ° 12 ′ 48" E 4 ° 40 ′ 50 " S , 39 ° 12 ′ 48" E
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Catchment area | about 7300 km² | |
Discharge at the Mwakijembe DS A Eo gauge : 7130 km² Location: 40 km above the mouth |
MNQ 1963-2002 MQ 1963-2002 Mq 1963-2002 MHQ 1963-2002 |
1 m³ / s 8 m³ / s 1.1 l / (s km²) 30 m³ / s |
Left tributaries | Mbalamu | |
Right tributaries | Mglumi; Bombo | |
Small towns | Lunga Lunga | |
Communities | Mlalo ; Lelwa; Mbuta; Rusanga; Duruma; Vanga |
The Umba is a river in northeast Tanzania in the Tanga region .
course
It rises in the Schageiu forest (Shagayu) in the West Usambara Mountains at an altitude of 2,000 m and flows eastwards on the northern side of the mountain range. The Mbalamu, which comes from the extreme north of the Usambara Mountains, and the Mglumi flow into the Umba at Lelwa. Shortly before it flows into the Indian Ocean , the Umba crosses the border into Kenya . The estuary itself marks the easternmost point of the border between Tanzania and Kenya, from which it was drawn in a largely straight line to the northwest in the 19th century towards Lake Victoria .
resources
In the mid-1960s, rich deposits of precious stones (especially sapphires and Spessartines ) were discovered on the upper reaches of the river . Also on the river is the Umba River Game Reserve , a game reserve that, together with the Mkomazi Reserve, covers approx. 2600 km² .
Hydrometry
Like most rivers in the region, the Umba flows depending on the rainy season. Average monthly flow through the Umba measured at the hydrological station at Mbuta, about 40 km above the mouth in m³ / s (1963–2003).
Individual evidence
- ^ A b Temporal Flow Variations: A Challenge for Water Management in Tanzania. Retrieved February 28, 2019 .
- ^ Deutsches Kolonial-Lexikon (1920), Volume III, p. 572. Accessed November 21, 2010 .